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Final Report
Time to lay down the law National legislation to enforce the BWC The Convention on the Prohibition of the Development, is the Verification Research, Training and Information Production and Stockpiling of Bacteriological (Biological) Centre, an independent, non-profit making, non-govern- Time to lay down the law and Toxin Weapons and on eir Destruction () obliges mental organisation. Its mission is to promote effective and states parties to take any necessary national measures to efficient verification as a means of ensuring confidence in National legislation to enforce the BWC implement the treaty in their territory. States parties have the implementation of international agreements and intra- agreed that this requires the adoption of legislation, including national agreements with international involvement. penal sanctions. aims to achieve its mission through research, training, Only now, thirty years after the treaty’s adoption, are states dissemination of information, and interaction with the parties collectively considering what legislative provisions relevant political, diplomatic, technical, scientific and non- are required to effectively enforce the treaty. This report is governmental communities. intended to assist states parties in this endeavour by assessing The Centre is based at Baird House, – St. Cross Street, the current status of their national legislation to enforce the London, , United Kingdom. treaty’s core prohibitions. The report provides comparative Phone +.()... analysis of existing legislation, makes recommendations for Fax +.()... increasing the rate of adoption of legislation and proposes E-mail [email protected] ways to make existing and new legislation more effective. Web www.vertic.org It should be of use to states parties preparing to adopt or amend legislation, states and organisations providing assist- Design and production: Richard Jones, Exile: Design and ance to states parties, and to the international community Editorial Services ([email protected]). -
Hnitflrcitilc
HNiTflRCiTilC A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) ,m — i * Halley, the British Antarctic Survey's station on the Brunt Ice Shelf, Coats Land,, was rebuilt last season for the third time since 1956-57. This picture taken in March shows one of the four wooden tubes, each of which houses a two-storey building, under construction in a pre-shaped and compacted snow hollow. BAS Copyngh! Registered at Post Office Headquarters, Vol. 10, No. 2 Wellington, New Zealand, as a magazine. SOUTH GEORGIA -.. SOUTH SANDWICH Is «C*2K SOUTH ORKNEY Is x \ 6SignyluK //o Orcadas arg SOUTH AMERICA / /\ ^ Borga T"^00Molodezhnaya \^' 4 south , * /weooEii \ ft SA ' r-\ *r\USSR --A if SHETLAND ,J£ / / ^^Jf ORONMIIDROWNING MAUD LAND' E N D E R B Y \ ] > * \ /' _ "iV**VlX" JN- S VDruzhnaya/General /SfA/ S f Auk/COATS ' " y C O A TBelirano SLd L d l arg L A N D p r \ ' — V&^y D««hjiaya/cenera.1 Beld ANTARCTIC •^W^fCN, uSS- fi?^^ /K\ Mawson \ MAC ROBERTSON LAN0\ \ *usi \ /PENINSULA' ^V^/^CRp^e J ^Vf (set mjp Mow) C^j V^^W^gSobralARG - Davis aust L Siple USA Amundsen-Scon OUEEN MARY LAND flMimy ELLSWORTH , U S A / ^ U S S R ') LAND °Vos1okussR/ r». / f c i i \ \ MARIE BYRO fee Shelf V\ . IAND WILKES LAND Scon ROSS|N2i? SEA jp>r/VICTORIAIj^V .TERRE ,; ' v / I ALAND n n \ \^S/ »ADEUL. n f i i f / / GEORGE V Ld .m^t Dumom d'Urville iranu Leningradskayra V' USSR,.'' \ -------"'•BAlLENYIs^ ANTARCTIC PENINSULA 1 Teniente Matienzo arc 2 Esperanza arg 3 Almirante Brown arg 4 Petrel arg 5 Decepcion arg 6 Vicecomodoro Marambio arg ' ANTARCTICA 7 Ariuro Prat chile 500 1000 Miles 8 Bernardo O'Higgms chile 9 Presidente Frei chile - • 1000 Kilomnre 10 Stonington I. -
Igneous Rocks of Peter I Island Hemisphere Tectonic Reconstructions
LeMasurier, W. E., and F. A. Wade. In press. Volcanic history in Marie Byrd Land: implications with regard to southern Igneous rocks of Peter I Island hemisphere tectonic reconstructions. In: Proceedings of the International Symposium on Andean and Antarctic Vol- canology Problems, Santiago, Chile (0. Gonzalez-Ferran, edi- tor). Rome, International Association of Volcanology and Chemistry of Earths Interior. THOMAS W. BASTIEN Price, R. C., and S. R. Taylor. 1973. The geochemistry of Dune- Ernest E. Lehmann Associates din Volcano, East Otago, New Zealand: rare earth elements. Minneapolis, Minnesota 55403 Contributions to Mineralogy and Petrology, 40: 195-205. Sun, S. S., and G. N. Hanson. 1975. Origin of Ross Island basanitoids and limitations upon the heterogeneity of mantle CAMPBELL CRADDOCK sources of alkali basalts and nephelinites. Contributions to Department of Geology and Geophysics Mineralogy and Petrology, 52: 77-106. The University of Wisconsin, Madison Sun, S. S., and G. N. Hanson. 1976. Rare earth element evi- Madison, Wisconsin 53706 dence for differentiation of McMurdo volcanics, Ross Island, Antarctica. Contributions to Mineralogy and Petrology, 54: 139-155. Peter I Island lies in the southeastern Pacific Ocean at 68°50S. 90°40W. about 240 nautical miles off the Eights Coast of West Antarctica. Ris- ing from the continental rise, it is one of the few truly oceanic islands in the region. Few people have been on the island, and little is known of its geology. Thaddeus von Bellingshausen discovered and named the island in 1821, and it was not seen again until sighted by Pierre Charcot in 1910. A Nor- wegian ship dredged some rocks off the west coast in 1927, and persons from the Norvegia achieved the first landing in 1929. -
National Report Norway
HCA9-07.4Ad IHO HYDROGRAPHIC COMMITTEE ON ANTARCTICA (HCA) 9th Meeting, Simon’s Town, Cape Town, South Africa, 12-14 October 2009 NATIONAL REPORT – NORWAY NORWEGIAN HYDROGRAPHIC SERVICE (NHS) 1. General The Norwegian Hydrographic Service (NHS) is responsible for the provision of hydrographic services for Norwegian waters and sea areas, including the Svalbard and Jan Mayen area. In Antarctica the Norwegian geographical area of interest mainly is concentrated in Dronning Maud Land (Queen Maud Land) and the adjacent Kong Håkon VII Hav (King Håkon VII Sea). Peter I Øy (Peter I Island) in the Bellingshausen Sea and Bouvetøya (Bouvet Island) are also Norwegian dependencies. However, the latter is north of the 60 parallel. In July 2008, Norway reached the goal of full ENC coverage for the Norwegian coast. Although this was a major step forwards, there still remains large areas with old data that needs to be replaced with new survey data. In addition, large areas on Svalbard remain to be surveyed and covered with ENCs and papercharts. The NHS has established a fully digital production flowline and all new products and updates are produced from a seamless Primary database. A new chart production system that enables more efficient maintenance of the ENC and chart portfolio is currently being fully implemented. The NHS intends to establish a Tracing service in 2009 and Print on Demand in 2010. Two projects are being carried out in order to develop the services including the technology needed to support it. PRIMAR International ENC service, operated by the Norwegian Hydrographic Service, now includes approx 8400 ENCs from more than 35 countries. -
Argentine and Chilean Claims to British Antarctica. - Bases Established in the South Shetlands
Keesing's Record of World Events (formerly Keesing's Contemporary Archives), Volume VI-VII, February, 1948 Argentine, Chilean, British, Page 9133 © 1931-2006 Keesing's Worldwide, LLC - All Rights Reserved. Argentine and Chilean Claims to British Antarctica. - Bases established in the South Shetlands. - Chilean President inaugurates Chilean Army Bases on Greenwich Island. - Argentine Naval Demonstration in British Antarctic Waters. - H.M.S. "Nigeria" despatched to Falklands. - British Government Statements. - Argentine-Chilean Agreement on Joint Defence of "Antarctic Rights." - The Byrd and Ronne Antarctic Expeditions. - Australian Antarctic Expedition occupies Heard Islands. The Foreign-Office in London, in statements on Feb. 7 and Feb. 13, announced that Argentina and Chile had rejected British protests, earlier presented in Buenos Aires and Santiago, against the action of those countries in establishing bases in British Antarctic territories. The announcement of Feb. 7 stated that on Dec. 7, 1947, the British Ambassador in Buenos Aires, Sir Reginald Leeper, had presented a Note expressing British "anxiety" at the activities in the Antarctic of an Argentine naval expedition which had visited part of the Falkland Islands Dependencies, including Graham Land, the South Shetlands, and the South Orkneys, and had landed at various points in British territory; that a request had been made for Argentine nationals to evacuate bases established on Deception Island and Gamma Island, in the South Shetlands; that H.M. Government had proposed that the Argentine should submit her claim to Antarctic sovereignty to the International Court of Justice for adjudication; and that on Dec. 23, 1947, a second British Note had been presented expressing surprise at continued violations of British territory and territorial waters by Argentine vessels in the Antarctic. -
Jane Francis British Antarctic Survey
Pliocene environments on Antarctica from the fossil record Jane Francis British Antarctic Survey J.Francis NASA Fossil plants in Antarctic rocks highlight past warm climates <1% rock but with fossils Seymour Island, Antarctica J.Francis Ron Blakey maps From 100 million years ago (Cretaceous) the Antarctic continent was over the South Pole………… but Antarctica was warm and green Cretaceous petrified tree stumps in their original growth position Alexander Island, Antarctica petrified tree trunk Fossil tree encased in rock strata fossil soil Jodie Howe Fossil pollen, fossil leaves and fossil wood Ferns Fossil Cladophlebis Dicksonia antarctica Monkey Puzzle trees grew in Antarctica J.Francis Araucaria araucana, Monkey Puzzle, growing today in the Chilean Andes Araucaria araucana R. Carpenter 100 million year old forests, Alexander Island Based on PhD work of Jodie Howe & Jane Francis, University of Leeds and BAS geologists. Painted by Rob Nicholls. Housed at BAS Tosolini, Francis, Cantrill Many Antarctic fossil plants are related to plants that live today in South America, Australia and New Zealand - ancient ancestors of Southern Hemisphere vegetation under warm climates Nothofagus Embothrium Brachychiton Cool temp Warm temp Sub-tropical Antarctica 70 million years ago ©James McKay Ross McPhee, American Museum of Natural History Antarctica 50 million years ago (Eocene) – very warm Cooler climates allowed ice sheets to form and glaciers reached the coast by 40 million years ago Reconstruction of Miocene ice sheet, Antarctica. 14-23 my Gasson -
Late Quaternary Environmental Changes in Marguerite Bay, Antarctic Peninsula, Inferred from Lake Sediments and Raised Beaches
Quaternary Science Reviews 68 (2013) 216e236 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Late Quaternary environmental changes in Marguerite Bay, Antarctic Peninsula, inferred from lake sediments and raised beaches Dominic A. Hodgson a,*,1, Stephen J. Roberts a,1, James A. Smith a, Elie Verleyen b, Mieke Sterken b, Minke Labarque b, Koen Sabbe b, Wim Vyverman b, Claire S. Allen a, Melanie J. Leng c, Charlotte Bryant d a NERC British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK b Department of Biology, Section of Protistology and Aquatic Ecology, University of Ghent, Krijgslaan 281 S8, 9000 Gent, Belgium c NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK d NERC Radiocarbon Facility, Scottish Enterprise Technology Park, Rankine Avenue, East Kilbride, Scotland G75 OQF, UK article info abstract Article history: The Antarctic Peninsula is one of the fastest-warming regions on Earth, but its palaeoenvironmental Received 4 October 2012 history south of 63 latitude is relatively poorly documented, relying principally on the marine geological Received in revised form record and short ice cores. In this paper, we present evidence of late-Quaternary environmental change 30 January 2013 from the Marguerite Bay region combining data from lake sediment records on Horseshoe Island and Accepted 1 February 2013 Pourquoi-Pas Island, and raised beaches at Horseshoe Island, Pourquoi-Pas Island and Calmette Bay. Lake Available online 27 March 2013 sediments were radiocarbon dated and analysed using a combination of sedimentological, geochemical and microfossil methods. Raised beaches were surveyed and analysed for changes in clast composition, Keywords: Antarctic Peninsula size and roundness. -
Oceans, Antarctica
G9102 ATLANTIC OCEAN. REGIONS, NATURAL FEATURES, G9102 ETC. .G8 Guinea, Gulf of 2950 G9112 NORTH ATLANTIC OCEAN. REGIONS, BAYS, ETC. G9112 .B3 Baffin Bay .B34 Baltimore Canyon .B5 Biscay, Bay of .B55 Blake Plateau .B67 Bouma Bank .C3 Canso Bank .C4 Celtic Sea .C5 Channel Tunnel [England and France] .D3 Davis Strait .D4 Denmark Strait .D6 Dover, Strait of .E5 English Channel .F45 Florida, Straits of .F5 Florida-Bahamas Plateau .G4 Georges Bank .G43 Georgia Embayment .G65 Grand Banks of Newfoundland .G7 Great South Channel .G8 Gulf Stream .H2 Halten Bank .I2 Iberian Plain .I7 Irish Sea .L3 Labrador Sea .M3 Maine, Gulf of .M4 Mexico, Gulf of .M53 Mid-Atlantic Bight .M6 Mona Passage .N6 North Sea .N7 Norwegian Sea .R4 Reykjanes Ridge .R6 Rockall Bank .S25 Sabine Bank .S3 Saint George's Channel .S4 Serpent's Mouth .S6 South Atlantic Bight .S8 Stellwagen Bank .T7 Traena Bank 2951 G9122 BERMUDA. REGIONS, NATURAL FEATURES, G9122 ISLANDS, ETC. .C3 Castle Harbour .C6 Coasts .G7 Great Sound .H3 Harrington Sound .I7 Ireland Island .N6 Nonsuch Island .S2 Saint David's Island .S3 Saint Georges Island .S6 Somerset Island 2952 G9123 BERMUDA. COUNTIES G9123 .D4 Devonshire .H3 Hamilton .P3 Paget .P4 Pembroke .S3 Saint Georges .S4 Sandys .S5 Smiths .S6 Southampton .W3 Warwick 2953 G9124 BERMUDA. CITIES AND TOWNS, ETC. G9124 .H3 Hamilton .S3 Saint George .S6 Somerset 2954 G9132 AZORES. REGIONS, NATURAL FEATURES, G9132 ISLANDS, ETC. .A3 Agua de Pau Volcano .C6 Coasts .C65 Corvo Island .F3 Faial Island .F5 Flores Island .F82 Furnas Volcano .G7 Graciosa Island .L3 Lages Field .P5 Pico Island .S2 Santa Maria Island .S3 Sao Jorge Island .S4 Sao Miguel Island .S46 Sete Cidades Volcano .T4 Terceira Island 2955 G9133 AZORES. -
Global Southern Limit of Flowering Plants and Moss Peat Accumulation Peter Convey,1 David W
RESEARCH/REVIEW ARTICLE Global southern limit of flowering plants and moss peat accumulation Peter Convey,1 David W. Hopkins,2,3,4 Stephen J. Roberts1 & Andrew N. Tyler3 1 British Antarctic Survey, National Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK 2 Scottish Crop Research Institute, Invergowrie, Dundee DD2 5DA, UK 3 Environmental Radioactivity Laboratory, School of Biological and Environmental Sciences, University of Stirling, Stirling FK9 4LA, UK 4 School of Life Sciences, Heriot-Watt University, Riccarton, Edinburgh EH14 4AS, UK Keywords Abstract Antarctic plants; distribution limits; peat accumulation; dating. The ecosystems of the western Antarctic Peninsula, experiencing amongst the most rapid trends of regional climate warming worldwide, are important ‘‘early Correspondence warning’’ indicators for responses expected in more complex systems else- Peter Convey, British Antarctic Survey, where. Central among responses attributed to this regional warming are National Environment Research Council, widely reported population and range expansions of the two native Antarctic High Cross, Madingley Road, Cambridge flowering plants, Deschampsia antarctica and Colobanthus quitensis. However, CB3 0ET, UK. E-mail: [email protected] confirmation of the predictions of range expansion requires baseline knowl- edge of species distributions. We report a significant southwards and westwards extension of the known natural distributions of both plant species in this region, along with several range extensions in an unusual moss community, based on a new survey work in a previously unexamined and un-named low altitude peninsula at 69822.0?S71850.7?W in Lazarev Bay, north-west Alexander Island, southern Antarctic Peninsula. These plant species therefore have a significantly larger natural range in the Antarctic than previously thought. -
Short Title Iota Reference Number List
RSGB IOTA DIRECTORY ANNEX F - SHORT TITLE IOTA REFERENCE NUMBER LIST AFRICA IOTA Ref Prefix IOTA Island Group IOTA Ref Prefix IOTA Island Group AF-001 3B6 Agalega Islands AF-066 C9 Gaza/Maputo District group AF-002 FT*Z Amsterdam & St Paul Islands AF-067 5Z Coast Province South group AF-003 ZD8 Ascension Island AF-068 CN, S0 Western Sahara South group AF-004 EA8 Canary Islands AF-069 EA9 Alhucemas Island AF-005 D4 Cape Verde – Leeward Islands AF-070 V5 Karas Region group AF-006 VQ9 Diego Garcia Island AF-071 Deleted Number AF-007 D6 Comoro Islands AF-072 C9 Inhambane District group AF-008 FT*W Crozet Islands AF-073 3V Sfax Region group AF-009 FT*E Europa Island AF-074 5H Lindi/Mtwara Region group AF-010 3C Bioco (Fernando Poo) Island AF-075 5H Dar Es Salaam/Pwani Region group AF-011 FT*G Glorioso Islands AF-076 5N Bayelsa/Rivers/Akwa Ibom etc States gp AF-012 FT*J Juan De Nova Island AF-077 ZS Western Cape Province South group AF-013 5R Madagascar (Main Island Only) AF-078 6W Senegal South group AF-014 CT3 Madeira Archipelago AF-079 ZS Eastern Cape Province group AF-015 3B7 Saint Brandon Islands AF-080 E3 Red Sea Coast North group AF-016 FR Reunion Island AF-081 E3 Red Sea Coast South group AF-017 3B9 Rodrigues Island AF-082 3C Rio Muni Province group AF-018 IH9 Pantelleria Island AF-083 3V Gabes/Medenine Region group AF-019 IG9 Pelagie Islands AF-084 9G Ghana group AF-020 J5 Bijagos Archipelago AF-085 ZS Western Cape Province North West group AF-021 ZS8 Prince Edward & Marion Islands AF-086 D4 Cape Verde – Windward Islands AF-022 ZD7 -
A Comparison of the Ammonite Faunas of the Antarctic Peninsula and Magallanes Basin
J. geol. Soc. London, Vol. 139, 1982, pp. 763-770, 1 fig, 1 table. Printed in Northern Ireland A comparison of the ammonite faunas of the Antarctic Peninsula and Magallanes Basin M. R. A. Thomson SUMMARY: Ammonite-bearingJurassic and Cretaceous sedimentary successions are well developed in the Antarctic Peninsula and the Magallanes Basin of Patagonia. Faunas of middle Jurassic-late Cretaceous age are present in Antarctica but those of Patagonia range no earlier than late Jurassic. Although the late Jurassic perisphinctid-dominated faunas of the Antarctic Peninsulashow wide-ranging Gondwana affinities, it is not yet possible to effect a close comparison with faunas of similar age in Patagonia because of the latter's poor preservation and our scant knowledge of them. In both regions the Neocomian is not well represented in the ammonite record, although uninterrupted sedimentary successions appear to be present. Lack of correspondence between the Aptian and Albian faunas of Alexander I. and Patagonia may be due to major differences in palaeogeographical setting. Cenomanian-Coniacian ammonite faunas are known only from Patagonia, although bivalve faunas indicate that rocks of this age are present in Antarctica. Kossmaticeratid faunas mark the late Cretaceous in both regions. In Antarcticathese have been classified as Campanian, whereas in Patagonia it is generally accepted, perhaps incorrectly, that these also range into the Maestrichtian. Fossiliferous Jurassic and Cretaceous marine rocks are rize first those of the Antarctic Peninsula and then to well developedin theAntarctic Peninsula, Scotia compare them with those of Patagonia. Comparisons Ridge andPatagonia (Fig. 1A).In Antarcticathese between Antarctic ammonite faunas and other Gond- rocks are distributed along the western and eastern wana areas wereoutlined by Thomson (1981a), and margins of theAntarctic Peninsula, formerly the the faunas of the marginal basin were discussed in magmatic arc from which the sediments were derived. -
History of Antarctica - Wikipedia, the Free Encyclopedia Page 1 of 13
History of Antarctica - Wikipedia, the free encyclopedia Page 1 of 13 Coordinates: 67°15′S 39°35′E History of Antarctica From Wikipedia, the free encyclopedia For the natural history of the Antarctic continent, see Antarctica. The history of Antarctica emerges from early Western theories of a vast continent, known as Terra Australis, believed to exist in the far south of the globe. The term Antarctic, referring to the opposite of the Arctic Circle, was coined by Marinus of Tyre in the 2nd century AD. The rounding of the Cape of Good Hope and Cape Horn in the 15th and 16th centuries proved that Terra Australis Incognita ("Unknown Southern Land"), if it existed, was a continent in its own right. In 1773 James Cook and his crew crossed the Antarctic Circle for the first time but although they discovered nearby islands, they did not catch sight of Antarctica itself. It is believed he was as close as 150 miles from the mainland. In 1820, several expeditions claimed to have been the first to have sighted the ice shelf or the continent. A Russian expedition was led by Fabian Gottlieb von Bellingshausen and Mikhail Lazarev, a British expedition was captained by Edward Bransfield and an American sealer Nathaniel Palmer participated. The first landing was probably just over a year later when American Captain John Davis, a sealer, set foot on the ice. Several expeditions attempted to reach the South Pole in the early 20th century, during the 'Heroic Age of Antarctic Exploration'. Many resulted in injury and death. Norwegian Roald Amundsen finally reached the Pole on December 14, 1911, following a dramatic race with the Englishman Robert Falcon Scott.